δ¹³C and δ¹⁸O limestone records as proxies for Mid-Carboniferous climate in Northwestern Mexico
Published: 16 September 2024| Version 1 | DOI: 10.17632/bm586r3r5x.1
Contributors:
Salvador Gutiérrez, Rafael Villanueva Olea, Pilar Navas-Parejo, Juan Moisés Casas PeñaDescription
δ¹³Ccarb and δ18Ocarb values in 38 limestone samples from the Mississippian-Pennsylvanian Boundary (MPB) cropping out in the Sierra Agua Verde, and 16 samples from the southwestern sector of Cerro Las Rastras, both located in Sonora, NW Mexico.
Files
Institutions
- Universidad Nacional Autonoma de Mexico
Categories
Paleoceanography, Limestone, Paleoclimate Proxy, Glaciation in Earth History, Mexico, Paleoclimatology, Paleozoic Era, Carboniferous Period, Pennsylvanian, Mississippian, Oxygen Isotope, Stable Isotope, Carbon Isotope
Funders
- CONAHCyTGrant ID: CF-7351
- UNAMGrant ID: UNAM-DGAPA-PAPIIT IN114923